North Atlantic Current variability through marine isotope stage M2 (circa 3.3 Ma) during the mid-Pliocene

Author:

De Schepper Stijn1,Head Martin J.2,Groeneveld Jeroen3

Affiliation:

1. Fachbereich Geowissenschaften; Universität Bremen; Bremen Germany

2. Department of Earth Sciences; Brock University; St. Catharines, Ontario Canada

3. MARUM; Universität Bremen; Bremen Germany

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference96 articles.

1. The deglaciation of the Northern Hemisphere: A global perspective;Alley;Annu. Rev. Earth Planet. Sci.,1999

2. Pliocene Discoaster abundance variations, Deep Sea Drilling Project Site 606: Biochronology and paleoenvironmental implications;Backman;Initial Rep. Deep Sea Drill. Proj.,1987

3. Quantitative biochronology of Pliocene and early Pleistocene calcareous nannofossils from the Atlantic, Indian and Pacific oceans;Backman;Mar. Micropaleontol.,1983

4. Dinoflagellate cysts in Upper Quaternary sediments from southwestern Norway and potential correlations with the oceanic record;Bakken;Boreas,1986

5. Magnetostratigraphic and biostratigraphic synthesis, Deep Sea Drilling Project Leg 94;Baldauf;Initial Rep. Deep Sea Drill. Proj.,1987

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